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Introduction to Vines and Wines

              Hort/VE 113 Fall 2012
            Session 6 -Grape Growing:
  climate and environment(cont.) Geology and Soils




Relative Cold Hardiness
        Low         Moderate              High
Chenin blanc     Sauvignon        Riesling
                 blanc
Merlot           Lemberger        Chardonnay
Sangiovese       Cabernet         Gewurztraminer
                 sauvignon
Semillon         Cabernet         Pinot noir
                 franc
Syrah                             Pinot gris
Viognier                          Pinot blanc




Relative Heat Requirements
      Low        Moderate              High
Riesling         Chardonnay Sauvignon blanc
Gewurztraminer Lemberger       Cabernet franc
Pinot noir       Merlot        Semillon
Pinot blanc      Syrah         Cabernet sauvignon
Pinot gris                     Sangiovese
                               Chenin blanc




                                                     1
http://www.youtube.com/wa
  tch?v=sVaZFCzxx24&playn
  ext=1&list=PLAC8CA53A2E
  20D3DD&feature=results_vi
  deo




                 Geology vs Soil

• Geology                     • Soil


• Study of the Earth          • A natural body comprised
                                of solids (minerals and
• The materials of which it     organic matter), liquid, and
  is made                       gases
• The structure of those      • Occurs on the land surface
  materials                   • Has horizons, or layers,
• and the processes acting      that are distinguishable
  upon them                     from the parent material
                              • As a result of additions,
                                losses, transfers, and
                                transformations




Geologic materials and processes
 are the building blocks upon which
 soils are formed

Vineyards grow on soils

Soils influence grape yield and
 quality




                                                               2
Igneous Rocks




Sedimentary Rocks




                    3
Metamorphic Rocks




       SOIL FORMATION
  Geologic materials
             on
  Landscapes
             are weathered by
  Climate
             under i fl
               d influence of
                            f
  Vegetation
             over eons of
  Time
              to form

              Soils




GEOLOGY AND SOILS

   Courtesy of:
   Joan Davenport
   Soil Scientist
   WSU-Prosser
   jdavenp@wsu.edu




                                4
Where in the
                                  World?




     Unique Pleistocene History of
            Columbia Basin
Event                    Result
Episodes of Glaciation   Sculpting of W. Canada &
                         PNW US; bouldery soil
                         materials




     Unique Pleistocene History of
            Columbia Basin
Event                     Result
Episodes of Glaciation    Sculpting of W. Canada
                          & PNW US; bouldery soil
                          materials
“Cataclysmic” Glacial     Channeled Scabland
Outburst Floods




                                                    5
Unique Pleistocene History of
          Columbia Basin
Event                    Result
Episodes of Glaciation   Sculpting of W. Canada
                         & PNW US; bouldery soil
                         materials
“Cataclysmic” Glacial    Channeled Scabland
Outburst Floods
Strong Directional       Dune fields and Palouse
Winds                    loess




   Unique Pleistocene History of
          Columbia Basin
Event                    Result
Episodes of Glaciation   Sculpting of W. Canada
                         & PNW US; bouldery soil
                         materials
“Cataclysmic” Glacial    Channeled Scabland
Outburst Floods
Strong Directional       Dune fields and Palouse
Winds                    loess
                         High Cascades; ash
Volcanic Eruptions       added to soils




               Glaciation




                                                   6
7
Cataclysmic Floods




                     8
9
Wind




       10
Strong Winds Spring and Fall




                       Prevailing strong
                       winds from SW




    Volcanic
    Eruptions




                                           11
May 17, 1980




                                May 18, 1980




Photos courtesy: USGS




                        Mount Mazama before
                             8000 yr BP
                         (no photo available)




                                 Mount Mazama
                               after 8000 yr BP




                                                  12
Mean Annual Precipitation




              Soils of Washington




Inceptisols
  & others

                    Spodosols                 Mollisols
         Ultisols   & Andisols

                                 Aridisols
                                 & Entisols




                                                          13
14
Generalized Soil Properties Important for
               Wine Grape

• Depth
• Texture & Structure
• Available water holding capacity
• Drainage
• Chemical Properties
• Quality (om, biota)
• Spatial variability




Soil Depth
•Important for root zone
 •depth of root penetration
 •water holding capacity
  d
 •drainage
 •nutrient holding capacity




       Site Potential (R. Smart)
• Based on depth of potential root zone

   • high       > 1m
   • medium     0.5
                05-1m
   • low        < 0.5 m




                                            15
Soil Texture

• % Sand (S)
  0.05 - 2.0 mm
• % Silt    (Si)
  0.002 - 0.05 mm
• % Clay (C)
  < 0.002 mm




                Soil Texture
• % Sand (S)
  0.05 - 2.0 mm
• % Silt    (Si)
  0.002 0.05
  0 002 - 0 05 mm
• % Clay (C)
  < 0.002 mm




                               16
Soil Textural Gradient

In general, soils
in central WA
are sandy close
to the i
t th river and d
become more fine
when moving
inland.




    Soil as a three phase system




               liquid       gas


                    solid




                                   17
void
                 gas           liquid

        solid          solid




VOIDS (Pores)
•Macropores
 •mostly air
•Micropores
 •mostly water
      l




                                        18
Soils
•Well drained generally best
 •Mixtures of sand, gravel, organic matter
•Drainage can be improved with drainage
 tile
 til
•Many wines benefit from the mineral
 content of the soil– sometimes chalky
•Rootstocks are selected for soil
 characteristics (texture, pH)




Thank you Dr. Davenport!




• http://wine.wsu.edu/faculty/joan-davenport


•   /




                                               19

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Wine lect6

  • 1. Introduction to Vines and Wines Hort/VE 113 Fall 2012 Session 6 -Grape Growing: climate and environment(cont.) Geology and Soils Relative Cold Hardiness Low Moderate High Chenin blanc Sauvignon Riesling blanc Merlot Lemberger Chardonnay Sangiovese Cabernet Gewurztraminer sauvignon Semillon Cabernet Pinot noir franc Syrah Pinot gris Viognier Pinot blanc Relative Heat Requirements Low Moderate High Riesling Chardonnay Sauvignon blanc Gewurztraminer Lemberger Cabernet franc Pinot noir Merlot Semillon Pinot blanc Syrah Cabernet sauvignon Pinot gris Sangiovese Chenin blanc 1
  • 2. http://www.youtube.com/wa tch?v=sVaZFCzxx24&playn ext=1&list=PLAC8CA53A2E 20D3DD&feature=results_vi deo Geology vs Soil • Geology • Soil • Study of the Earth • A natural body comprised of solids (minerals and • The materials of which it organic matter), liquid, and is made gases • The structure of those • Occurs on the land surface materials • Has horizons, or layers, • and the processes acting that are distinguishable upon them from the parent material • As a result of additions, losses, transfers, and transformations Geologic materials and processes are the building blocks upon which soils are formed Vineyards grow on soils Soils influence grape yield and quality 2
  • 4. Metamorphic Rocks SOIL FORMATION Geologic materials on Landscapes are weathered by Climate under i fl d influence of f Vegetation over eons of Time to form Soils GEOLOGY AND SOILS Courtesy of: Joan Davenport Soil Scientist WSU-Prosser jdavenp@wsu.edu 4
  • 5. Where in the World? Unique Pleistocene History of Columbia Basin Event Result Episodes of Glaciation Sculpting of W. Canada & PNW US; bouldery soil materials Unique Pleistocene History of Columbia Basin Event Result Episodes of Glaciation Sculpting of W. Canada & PNW US; bouldery soil materials “Cataclysmic” Glacial Channeled Scabland Outburst Floods 5
  • 6. Unique Pleistocene History of Columbia Basin Event Result Episodes of Glaciation Sculpting of W. Canada & PNW US; bouldery soil materials “Cataclysmic” Glacial Channeled Scabland Outburst Floods Strong Directional Dune fields and Palouse Winds loess Unique Pleistocene History of Columbia Basin Event Result Episodes of Glaciation Sculpting of W. Canada & PNW US; bouldery soil materials “Cataclysmic” Glacial Channeled Scabland Outburst Floods Strong Directional Dune fields and Palouse Winds loess High Cascades; ash Volcanic Eruptions added to soils Glaciation 6
  • 7. 7
  • 9. 9
  • 10. Wind 10
  • 11. Strong Winds Spring and Fall Prevailing strong winds from SW Volcanic Eruptions 11
  • 12. May 17, 1980 May 18, 1980 Photos courtesy: USGS Mount Mazama before 8000 yr BP (no photo available) Mount Mazama after 8000 yr BP 12
  • 13. Mean Annual Precipitation Soils of Washington Inceptisols & others Spodosols Mollisols Ultisols & Andisols Aridisols & Entisols 13
  • 14. 14
  • 15. Generalized Soil Properties Important for Wine Grape • Depth • Texture & Structure • Available water holding capacity • Drainage • Chemical Properties • Quality (om, biota) • Spatial variability Soil Depth •Important for root zone •depth of root penetration •water holding capacity d •drainage •nutrient holding capacity Site Potential (R. Smart) • Based on depth of potential root zone • high > 1m • medium 0.5 05-1m • low < 0.5 m 15
  • 16. Soil Texture • % Sand (S) 0.05 - 2.0 mm • % Silt (Si) 0.002 - 0.05 mm • % Clay (C) < 0.002 mm Soil Texture • % Sand (S) 0.05 - 2.0 mm • % Silt (Si) 0.002 0.05 0 002 - 0 05 mm • % Clay (C) < 0.002 mm 16
  • 17. Soil Textural Gradient In general, soils in central WA are sandy close to the i t th river and d become more fine when moving inland. Soil as a three phase system liquid gas solid 17
  • 18. void gas liquid solid solid VOIDS (Pores) •Macropores •mostly air •Micropores •mostly water l 18
  • 19. Soils •Well drained generally best •Mixtures of sand, gravel, organic matter •Drainage can be improved with drainage tile til •Many wines benefit from the mineral content of the soil– sometimes chalky •Rootstocks are selected for soil characteristics (texture, pH) Thank you Dr. Davenport! • http://wine.wsu.edu/faculty/joan-davenport • / 19